Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland
C23B-0603 Ilulissat Icefjord in West-Greenland is the fastest and most productive iceberg calving area outside Antarctica. Changes in climate exert a first-order control on the recession of the icefront and the calving of the icebergs. Glacial and geological processes related to iceberg calving and...
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ftoceanrep:oai:oceanrep.geomar.de:10855 2023-05-15T13:47:22+02:00 Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland Schumann, Kai Weinrebe, Wilhelm Völker, David Kuijpers, Antoon 2010 https://oceanrep.geomar.de/id/eprint/10855/ http://www.agu.org/cgi-bin/SFgate/SFgate?language=English&verbose=0&listenv=table&application=fm10&convert=&converthl=&refinequery=&formintern=&formextern=&transquery=ilulissat&_lines=&multiple=0&descriptor=%2fdata%2fepubs%2fwais%2findexes%2ffm10%2ffm10%7C6 unknown Schumann, K., Weinrebe, W., Völker, D. and Kuijpers, A. (2010) Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland. [Poster] In: AGU Fall Meeting 2010. , 13.12.-17.12.2010, San Francisco, California, USA . Conference or Workshop Item NonPeerReviewed 2010 ftoceanrep 2023-04-07T14:59:07Z C23B-0603 Ilulissat Icefjord in West-Greenland is the fastest and most productive iceberg calving area outside Antarctica. Changes in climate exert a first-order control on the recession of the icefront and the calving of the icebergs. Glacial and geological processes related to iceberg calving and transport shape the morphology of the seafloor in the area characteristically. Revealing the morphology by high-resolution bathymetric mapping helps to understand these processes. During a cruise with RV Maria S. Merian in summer 2007 large parts of the area were mapped with Kongsberg EM120 and EM1002 multibeam systems. This data was complemented by a survey using a portable Seabeam 1180 multibeam system temporarily mounted on the small local vessel Smilla which could navigate through areas inside the icefjord inaccessible to large research vessels. A comprehensive image of the morphology of the area was achieved by compiling and merging both datasets. Different morphological features such as ridges, shaped like drumlins and valleys which could be connected to channel systems, directing debris flows to a deposition centre characterize the central part of the survey area. Here, a series of prominent circular features 80m to 150m in diameter and up to 30m deep have been found and are interpreted as pockmarks. A parasound sediment echosounder profile across one of the pockmarks documents the absence of the upper sedimentary unit inside. Furthermore, a blank zone in the central part indicates uprising fluids or gas. The northeast - southwest alignment of the pockmarks points to a formation related to slides, faults, and iceberg furrows. The depth of their occurrence indicates a formation by dissociating gas hydrates. The most recent active pockmarks are located in the centre and the northeastern end of the depression in a depth of 395m. The gas hydrate stability zone in arctic regions tapers out at around 400m at 3° bottom water temperature which coincides with the values measured with a CTD close to this position. The ... Conference Object Antarc* Antarctica Arctic Greenland Iceberg* Ilulissat OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Greenland Ilulissat ENVELOPE(-51.099,-51.099,69.220,69.220) Kongsberg ENVELOPE(19.082,19.082,69.123,69.123) |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
unknown |
description |
C23B-0603 Ilulissat Icefjord in West-Greenland is the fastest and most productive iceberg calving area outside Antarctica. Changes in climate exert a first-order control on the recession of the icefront and the calving of the icebergs. Glacial and geological processes related to iceberg calving and transport shape the morphology of the seafloor in the area characteristically. Revealing the morphology by high-resolution bathymetric mapping helps to understand these processes. During a cruise with RV Maria S. Merian in summer 2007 large parts of the area were mapped with Kongsberg EM120 and EM1002 multibeam systems. This data was complemented by a survey using a portable Seabeam 1180 multibeam system temporarily mounted on the small local vessel Smilla which could navigate through areas inside the icefjord inaccessible to large research vessels. A comprehensive image of the morphology of the area was achieved by compiling and merging both datasets. Different morphological features such as ridges, shaped like drumlins and valleys which could be connected to channel systems, directing debris flows to a deposition centre characterize the central part of the survey area. Here, a series of prominent circular features 80m to 150m in diameter and up to 30m deep have been found and are interpreted as pockmarks. A parasound sediment echosounder profile across one of the pockmarks documents the absence of the upper sedimentary unit inside. Furthermore, a blank zone in the central part indicates uprising fluids or gas. The northeast - southwest alignment of the pockmarks points to a formation related to slides, faults, and iceberg furrows. The depth of their occurrence indicates a formation by dissociating gas hydrates. The most recent active pockmarks are located in the centre and the northeastern end of the depression in a depth of 395m. The gas hydrate stability zone in arctic regions tapers out at around 400m at 3° bottom water temperature which coincides with the values measured with a CTD close to this position. The ... |
format |
Conference Object |
author |
Schumann, Kai Weinrebe, Wilhelm Völker, David Kuijpers, Antoon |
spellingShingle |
Schumann, Kai Weinrebe, Wilhelm Völker, David Kuijpers, Antoon Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland |
author_facet |
Schumann, Kai Weinrebe, Wilhelm Völker, David Kuijpers, Antoon |
author_sort |
Schumann, Kai |
title |
Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland |
title_short |
Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland |
title_full |
Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland |
title_fullStr |
Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland |
title_full_unstemmed |
Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland |
title_sort |
indications of gas-hydrate dissociation caused by sea level rise off ilulissat icefjord, greenland |
publishDate |
2010 |
url |
https://oceanrep.geomar.de/id/eprint/10855/ http://www.agu.org/cgi-bin/SFgate/SFgate?language=English&verbose=0&listenv=table&application=fm10&convert=&converthl=&refinequery=&formintern=&formextern=&transquery=ilulissat&_lines=&multiple=0&descriptor=%2fdata%2fepubs%2fwais%2findexes%2ffm10%2ffm10%7C6 |
long_lat |
ENVELOPE(-51.099,-51.099,69.220,69.220) ENVELOPE(19.082,19.082,69.123,69.123) |
geographic |
Arctic Greenland Ilulissat Kongsberg |
geographic_facet |
Arctic Greenland Ilulissat Kongsberg |
genre |
Antarc* Antarctica Arctic Greenland Iceberg* Ilulissat |
genre_facet |
Antarc* Antarctica Arctic Greenland Iceberg* Ilulissat |
op_relation |
Schumann, K., Weinrebe, W., Völker, D. and Kuijpers, A. (2010) Indications of gas-hydrate dissociation caused by sea level rise off Ilulissat Icefjord, Greenland. [Poster] In: AGU Fall Meeting 2010. , 13.12.-17.12.2010, San Francisco, California, USA . |
_version_ |
1766246976423198720 |